Geological Bulletin, Volume 12University of Peshawar, 1979 - Geology |
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Page 14
It is also observed that the carbonate minerals are more prominant in the basal
part as compared to the upper part . However , no gradual change is observed .
Recrystallization of the carbonate minerals is also an important textural feature ...
It is also observed that the carbonate minerals are more prominant in the basal
part as compared to the upper part . However , no gradual change is observed .
Recrystallization of the carbonate minerals is also an important textural feature ...
Page 17
The view is further confirmed by the fact that glauconite is present only in the very
basal part of the formation . Ore minerals Ore minerals are present in a minor
amount in the basal part but dominate the upper part and the shaly intercalations
.
The view is further confirmed by the fact that glauconite is present only in the very
basal part of the formation . Ore minerals Ore minerals are present in a minor
amount in the basal part but dominate the upper part and the shaly intercalations
.
Page 25
Traces of glauconite and a few ghost structures are noticed in the very basal part
of the formation . They are observed at levels containing little calcareous
minerals . Since they are absent from the rest of the formation , the writers
suggest that ...
Traces of glauconite and a few ghost structures are noticed in the very basal part
of the formation . They are observed at levels containing little calcareous
minerals . Since they are absent from the rest of the formation , the writers
suggest that ...
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Contents
1979 No | 1 |
Khewra Gorge Khewra Jehluu District | 11 |
Khewra Gorge Khewra Jehlum District | 21 |
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Common terms and phrases
abundant anhedral appears Baghanwala Formation basal base basin biotite brown Bull calcarenite calcareous calcareous cement calcite Cambrian carbonate carbonate and limonite carbonate minerals Cementing material characterized chlorite circulated clastic clay clear colour common Compactibility constituents contains corroded boundaries crystals cubic currents deposition dominant Early effects environments exposed field formed fossils Geol Geology glauconite important India indicate industries interbeddings intercalations iron oxide Jutana Dolomite KHAN Khewra Gorge laminated layers less limestone limonite maroon material is carbonate matrix medium metamorphism meters mica micaceous minerals noticed observed occurs olive origin Pakistan Peshawar pigmentation places porosity present primary pseudomorphs Punjab quartz grains recrystallized result ripple marks rocks rounded Saline Salt Range sand sandstone sector sedimentary sediments seen shale shallow slides solution strata stratification structures stylolites suggestive texture thick thin bedded Thin Section tion underlying Univ upper various vary warm writers York